Methods and systems for low frequency seismic and infrasound detection of geo-pressure transition zones
View Patent ↗Methods for determining the existence and characteristics of a gradational pressurized zone within a subterranean formation are disclosed. One embodiment involves employing an attenuation relationship between a seismic response signal and increasing wavelet wavelength, which relationship may be used to detect a gradational pressurized zone and/or determine characteristics thereof. In another embodiment, a method for analyzing data contained within a response signal for signal characteristics that may change in relation to the distance between an input signal source and the gradational pressurized zone is disclosed. In a further embodiment, the relationship between response signal wavelet frequency and comparative amplitude may be used to estimate an optimal wavelet wavelength or range of wavelengths used for data processing or input signal selection. Systems for seismic exploration and data analysis for practicing the above-mentioned method embodiments are also disclosed.
1. A method of performing seismic exploration to identify at least a presence of a gradational pressurized zone, comprising:
transmitting an input signal into a subterranean formation from one of a location proximate a drill bit at a distal end of a drill string and a location offset and remote from the distal end of the drill string;
receiving the input signal and a reflected signal comprising a response signal of the input signal at another of the location proximate the drill bit at the distal end of the drill string and the location offset and remote from the distal end of the drill string;
measuring the response signal; and
analyzing the response signal to identify at least a presence of a gradational pressurized zone in an intended path of the drill bit using an attenuation relationship comprising a comparative amplitude of the response signal to the input signal as representative of at least a presence of a gradational pressurized zone by relation of an amplitude of the response signal indicative of at least the presence of a gradational pressurized zone to at least one wavelength of the input signal;
wherein the attenuation relationship comprises:
A
c
=
(
.5
·
cos
(
2
·
π
·
T
g
λ
)
)
+
.5
where: A c is a comparative amplitude of the response signal to the input signal, T g is the thickness of the gradational pressurized zone, and λ is the at least one wavelength of the input signal.
2. The method of claim 1 , wherein transmitting an input signal comprises transmitting an input signal including a wavelength greater than about 250 feet.
3. The method of claim 1 , wherein transmitting an input signal comprises transmitting an input signal including a wavelength greater than about 500 feet.
4. The method of claim 1 , wherein transmitting an input signal comprises transmitting an input signal including a wavelength greater than about 2 times the thickness of a gradational pressurized zone encountered by the input signal.
5. The method of claim 1 , wherein analyzing the response signal comprises comparing a wavelet having a wavelength of less than 250 feet to a wavelet having a wavelength of more than 250 feet.
6. The method of claim 1 , wherein analyzing the response signal comprises comparing a wavelet having a wavelength of less than 2000 feet to a wavelet having a wavelength of more than 2000 feet.
7. The method of claim 1 , wherein analyzing the response signal comprises generating a wavelet having a wavelength greater than about 2 times the thickness of a gradational pressurized zone encountered by the input signal.
8. The method of claim 1 , wherein analyzing the response signal comprises comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength of about 2 times the first wavelength.
9. The method of claim 8 , wherein comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength comprises comparing a first wavelet having a wavelength of about 250 feet to a second wavelet having a second wavelength of about 500 feet.
10. The method of claim 8 , wherein comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength comprises comparing a first wavelet having a wavelength of about 500 feet to a second wavelet having a second wavelength of about 1000 feet.
11. The method of claim 8 , wherein comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength comprises comparing a first wavelet having a wavelength of about 1000 feet to a second wavelet having a second wavelength of about 2000 feet.
12. The method of claim 1 , further comprising selecting the location offset and remote from the distal end of the drill string to be a location at the surface of the earth.
13. A method of performing seismic exploration to identify a presence and estimate a thickness of at least a portion of a gradational pressurized zone, comprising:
transmitting an input signal into a subterranean formation from one of a location proximate a drill bit at a distal end of a drill string and a location offset and remote from the distal end of the drill string;
receiving the input signal and a reflected signal comprising a response signal of the input signal at another of the location proximate the drill bit at the distal end of the drill string and the location offset and remote from the distal end of the drill string;
measuring the response signal;
analyzing the response signal to identify a presence of at least a portion of a gradational pressurized zone in an intended path of the drill bit using an attenuation relationship comprising a comparative amplitude of the response signal to the input signal as representative of the presence of the at least a portion of the gradational pressurized zone by relation of an amplitude of the response signal indicative of the presence and the thickness of the gradational pressurized zone to at least one wavelength of the input signal
wherein the attenuation relationship comprises:
A
c
=
(
.5
·
cos
(
2
·
π
·
T
g
λ
)
)
+
.5
where: A c is a comparative amplitude of the response signal to the input signal, T g is the thickness of the gradational pressurized zone, and λ is the wavelength of the at least one input signal, for T g ; and
determining the thickness of the at least a portion of the identified gradational pressurized zone identified to be present responsive to analyzing the response signal.
14. A method of performing seismic exploration to identify at least a presence of a gradational pressurized zone, comprising:
transmitting an input signal into a subterranean formation;
measuring a response signal of the input signal;
analyzing the response signal using an attenuation relationship comprising:
A
c
=
(
.5
·
cos
(
2
·
π
·
T
g
λ
)
)
+
.5
where: A c is a comparative amplitude of a response signal to an input signal, T g is the thickness of the gradational pressurized zone, and λ is a wavelength of the input signal; and
identifying at least a presence of a gradational pressurized zone responsive to analyzing the response signal.
15. The method of claim 14 , wherein transmitting an input signal comprises transmitting an input signal including a wavelength greater than about 250 feet.
16. The method of claim 14 , wherein transmitting an input signal comprises transmitting an input signal including a wavelength greater than about 500 feet.
17. The method of claim 14 , wherein transmitting an input signal comprises transmitting an input signal including a wavelength greater than about 2 times the thickness of a gradational pressurized zone encountered by the input signal.
18. The method of claim 14 , wherein analyzing the response signal comprises comparing a wavelet having a wavelength of less than 250 feet to a wavelet having a wavelength of more than 250 feet.
19. The method of claim 14 , wherein analyzing the response signal comprises comparing a wavelet having a wavelength of less than 2000 feet to a wavelet having a wavelength of more than 2000 feet.
20. The method of claim 14 , wherein analyzing the response signal comprises generating a wavelet having a wavelength greater than about 2 times the thickness of a gradational pressurized zone encountered by the input signal.
21. The method of claim 14 , wherein analyzing the response signal comprises comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength of about 2 times the first wavelength.
22. The method of claim 21 , wherein comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength comprises comparing a first wavelet having a wavelength of about 250 feet to a second wavelet having a second wavelength of about 500 feet.
23. The method of claim 21 , wherein comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength comprises comparing a first wavelet having a wavelength of about 500 feet to a second wavelet having a second wavelength of about 1000 feet.
24. The method of claim 21 , wherein comparing a first wavelet having a first wavelength to a second wavelet having a second wavelength comprises comparing a first wavelet having a wavelength of about 1000 feet to a second wavelet having a second wavelength of about 2000 feet.
25. The method of claim 14 , further comprising determining at least one characteristic of the gradational pressurized zone identified to be present responsive to analyzing the response signal.
26. The method of claim 25 wherein identifying the at least one characteristic of a gradational pressurized zone identified to be present further comprises estimating the thickness of at least a portion of the gradational pressurized zone.
27. The method of claim 26 , wherein estimating the thickness of at least a portion of the gradational pressurized zone comprises solving the attenuation relationship.